Eddies in Marine Science:
It is now well known that the mid-ocean flow is almost everywhere domi nated by so-called synoptic or meso-scale eddies, rotating about nearly vertical axes and extending throughout the water column. A typical mid ocean horizontal scale is 100 km and a time scale is 100 days: these meso scale eddies...
Gespeichert in:
| Weitere Verfasser: | |
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| Format: | Elektronisch E-Book |
| Sprache: | English |
| Veröffentlicht: |
Berlin, Heidelberg
Springer Berlin Heidelberg
1983
|
| Schriftenreihe: | Topics in Atmospheric and Oceanographic Sciences
|
| Schlagworte: | |
| Online-Zugang: | BTU01 Volltext |
| Zusammenfassung: | It is now well known that the mid-ocean flow is almost everywhere domi nated by so-called synoptic or meso-scale eddies, rotating about nearly vertical axes and extending throughout the water column. A typical mid ocean horizontal scale is 100 km and a time scale is 100 days: these meso scale eddies have swirl speeds of order 10 cm s -1 which are usually con siderably greater than the long-term average flow. Many types of eddies with somewhat different scales and characteristics have been identified. The existence of such eddies was suspected by navigators more than a century ago and confirmed by the world of C. O'D. Iselin and V. B. Stock man in the 1930's. Measurements from RIV Aries in 1959/60, using the then newly developed neutrally buoyant floats, indicated the main char acteristics of the eddies in the deep ocean of the NW Atlantic while a se ries of Soviet moored current-meter arrays culminated, in POLYGON- 1970, in the explicit mapping of an energetic anticyclonic eddy in the tropical NE Atlantic. In 1973 a large collaborative (mainly U. S. , U. K. ) program, MODE-I, produced synoptic charts for an area of the NW At lantic and confirmed the existence of an open ocean eddy field and es tablished its characteristics. Meso-scale eddies are now known to be of interest and importance to marine chemists and biologists as well as to physical oceanographers and meteorologists |
| Beschreibung: | 1 Online-Ressource (XXVI, 612 p) |
| ISBN: | 9783642690037 |
| DOI: | 10.1007/978-3-642-69003-7 |
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| 520 | |a It is now well known that the mid-ocean flow is almost everywhere domi nated by so-called synoptic or meso-scale eddies, rotating about nearly vertical axes and extending throughout the water column. A typical mid ocean horizontal scale is 100 km and a time scale is 100 days: these meso scale eddies have swirl speeds of order 10 cm s -1 which are usually con siderably greater than the long-term average flow. Many types of eddies with somewhat different scales and characteristics have been identified. The existence of such eddies was suspected by navigators more than a century ago and confirmed by the world of C. O'D. Iselin and V. B. Stock man in the 1930's. Measurements from RIV Aries in 1959/60, using the then newly developed neutrally buoyant floats, indicated the main char acteristics of the eddies in the deep ocean of the NW Atlantic while a se ries of Soviet moored current-meter arrays culminated, in POLYGON- 1970, in the explicit mapping of an energetic anticyclonic eddy in the tropical NE Atlantic. In 1973 a large collaborative (mainly U. S. , U. K. ) program, MODE-I, produced synoptic charts for an area of the NW At lantic and confirmed the existence of an open ocean eddy field and es tablished its characteristics. Meso-scale eddies are now known to be of interest and importance to marine chemists and biologists as well as to physical oceanographers and meteorologists | ||
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Datensatz im Suchindex
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| discipline | Geologie / Paläontologie Physik |
| doi_str_mv | 10.1007/978-3-642-69003-7 |
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| illustrated | Not Illustrated |
| indexdate | 2024-07-10T08:10:45Z |
| institution | BVB |
| isbn | 9783642690037 |
| language | English |
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| series2 | Topics in Atmospheric and Oceanographic Sciences |
| spelling | Eddies in Marine Science edited by Allan R. Robinson Berlin, Heidelberg Springer Berlin Heidelberg 1983 1 Online-Ressource (XXVI, 612 p) txt rdacontent c rdamedia cr rdacarrier Topics in Atmospheric and Oceanographic Sciences It is now well known that the mid-ocean flow is almost everywhere domi nated by so-called synoptic or meso-scale eddies, rotating about nearly vertical axes and extending throughout the water column. A typical mid ocean horizontal scale is 100 km and a time scale is 100 days: these meso scale eddies have swirl speeds of order 10 cm s -1 which are usually con siderably greater than the long-term average flow. Many types of eddies with somewhat different scales and characteristics have been identified. The existence of such eddies was suspected by navigators more than a century ago and confirmed by the world of C. O'D. Iselin and V. B. Stock man in the 1930's. Measurements from RIV Aries in 1959/60, using the then newly developed neutrally buoyant floats, indicated the main char acteristics of the eddies in the deep ocean of the NW Atlantic while a se ries of Soviet moored current-meter arrays culminated, in POLYGON- 1970, in the explicit mapping of an energetic anticyclonic eddy in the tropical NE Atlantic. In 1973 a large collaborative (mainly U. S. , U. K. ) program, MODE-I, produced synoptic charts for an area of the NW At lantic and confirmed the existence of an open ocean eddy field and es tablished its characteristics. Meso-scale eddies are now known to be of interest and importance to marine chemists and biologists as well as to physical oceanographers and meteorologists Earth Sciences Geophysics/Geodesy Oceanography Earth sciences Geophysics Meeresströmung (DE-588)4130725-2 gnd rswk-swf Meeresströmung (DE-588)4130725-2 s 1\p DE-604 Robinson, Allan R. edt Erscheint auch als Druck-Ausgabe 9783642690051 https://doi.org/10.1007/978-3-642-69003-7 Verlag URL des Erstveröffentlichers Volltext 1\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk |
| spellingShingle | Eddies in Marine Science Earth Sciences Geophysics/Geodesy Oceanography Earth sciences Geophysics Meeresströmung (DE-588)4130725-2 gnd |
| subject_GND | (DE-588)4130725-2 |
| title | Eddies in Marine Science |
| title_auth | Eddies in Marine Science |
| title_exact_search | Eddies in Marine Science |
| title_full | Eddies in Marine Science edited by Allan R. Robinson |
| title_fullStr | Eddies in Marine Science edited by Allan R. Robinson |
| title_full_unstemmed | Eddies in Marine Science edited by Allan R. Robinson |
| title_short | Eddies in Marine Science |
| title_sort | eddies in marine science |
| topic | Earth Sciences Geophysics/Geodesy Oceanography Earth sciences Geophysics Meeresströmung (DE-588)4130725-2 gnd |
| topic_facet | Earth Sciences Geophysics/Geodesy Oceanography Earth sciences Geophysics Meeresströmung |
| url | https://doi.org/10.1007/978-3-642-69003-7 |
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